OCEAN BASINS
Ocean Basins
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Continental margin
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Deep sea floor
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Mid-ocean ridge
Continental Margins
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Passive
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Continental shelf
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shallow, flat, very gently sloping continental
area submerged by sea water
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composed of sediments overlying continental crust
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extension of the coastal plain
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Continental slope
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relatively steep (3° to 6°) area of continental
margin
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transition between continental shelf and rise
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Continental rise
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sedimentary apron at base of continental slope
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overlies transition between continental and oceanic
crust
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Active - continental margin bordering
a trench
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narrow continental shelf
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continental slope but no continental
rise - sediments dumped in trench
Continental Margins (cont.)
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Other features
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Submarine canyons
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cut by turbidity currents - very dilute slurries
of sediment and water
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Abyssal fan
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fan-shaped sedimentary deposit on continental
rise
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analogous to alluvial fan
Abyssal Fans
Deep Sea Floor
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Abyssal hills
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rough volcanic topography
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ocean in sediment-starved ocean
basins (Ex: Pacific Ocean)
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Abyssal plain
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flattest feature on Earth
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forms from sediment deposition
that buries rough volcanic features
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terrigenous sediment - sediment derived from
land
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pelagic sediment - sediment deposited far from
land; derived from marine organisms (coccoliths, foraminifera)
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terrigenous sediments deposited by turbidity
currents - turbidites
Deep Sea Floor (cont.)
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Mystery of the breaks in the Trans-Atlantic
telegraph cable
Deep Sea Floor (cont.)
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Abyssal plain
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where sedimentation is very slow
get manganese nodules
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potato sized nodules of Mn and Fe oxides
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grow very slowly (1 mm/m.y.)
Mid-Ocean Ridges
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Mid-Ocean Ridge
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Transform faults
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area between ridges where crust (and plates)
show relative motion
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Fracture zones
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chasm formed as a result of faulting
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Rift valley
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central valley in mid-ocean ridge
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tension causes down-faulting of blocks
Black smokers
Origin of Ocean Basins
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Rifting (Fig.
11-17a)
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rifting beginning; not flooded
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little or no basalt
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Ex: African Rift Valley, Imperial
Valley, CA
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Linear sea
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flooded with seawater but not true
ocean
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Ex: Red Sea, Gulf of California
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Mature ocean basin
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true ocean; still widening
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Ex: Atlantic Ocean
Decline of
Ocean Basins
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Declining ocean basin
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true ocean
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ringed by subduction zones; becoming
smaller
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Ex: Pacific Ocean
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Terminal ocean basin
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no longer a true ocean; subducted
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Ex: Mediterranean Sea